Abstract
Eight unacclimatized long-distance runners performed, on a level
treadmill, an incremental test to determine the maximal oxygen uptake
(V˙O2max) and the minimal velocity eliciting
V˙O2max (vV˙O2max) in normoxia (N) and acute
moderate hypoxia (H) corresponding to an altitude of 2400 m
(PIO2 of 109 mmHg). Afterwards, on separate days, they
performed two all-out constant velocity runs at vV˙O2max in a
random order (one in N and the other in H). The decrease in
V˙O2max between N and H showed a great degree of variability
amongst subjects as V˙O2max decreased by
8.9 ± 4 ml × min-1 × kg-1
in H vs. N conditions (-15.3 ± 6.3 % with a
range from -7.9 % to -23.8 %). This decrease in
V˙O2max was proportional to the value of V˙O2max
(V˙O2max vs. delta V˙O2max N-H,
r = 0.75, p = 0.03). The time run at
vV˙O2max was not affected by hypoxia
(483 ± 122 vs. 506 ± 148 s, in
N and H, respectively, p = 0.37). However, the greater the
decrease in vV˙O2max during hypoxia, the greater the runners
increased their time to exhaustion at vV˙O2max
(vV˙O2max N-H vs. tlim @vV˙O2max N-H,
r = -0.75, p = 0.03). In conclusion,
this study showed that there was a positive association between the extent of
decrease in vV˙O2max, and the increase in run time at
vV˙O2max in hypoxia.
Key words
Exercise - altitude - maximal oxygen uptake - fatigue
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